
Clean water is important for human life, and obtaining it with the least amount of energy is significant. This research aims to desalinate water using a horizontal multiple effects diffusion solar still (DSS). A small distillation device with an area of 10 × 10 cm2 was designed and 3D printed. An electric heater was used to simulate solar radiation at 400, 700, and 1000 W/m2. The amount of water produced when using 1, 3, and 5 effects was recorded. The most notable results were: maximum water yield reached 1.93 kg/m2 h at 1000 W/m2, at which the solar to vapor conversion efficiency was 107%. The daily water yields throughout the year were estimated, and the maximum production was 10.16 kg/m2 during a day in June, when the global horizontal irradiance was 7.01 kWh/m2. The results were also compared with other distillation systems.
Citation: Abdulrahman Almutlaq. Indoor experiments of a horizontal multiple effects diffusion solar still: Influence of heat input and the number of stages[J]. AIMS Energy, 2024, 12(2): 532-547. doi: 10.3934/energy.2024025
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Clean water is important for human life, and obtaining it with the least amount of energy is significant. This research aims to desalinate water using a horizontal multiple effects diffusion solar still (DSS). A small distillation device with an area of 10 × 10 cm2 was designed and 3D printed. An electric heater was used to simulate solar radiation at 400, 700, and 1000 W/m2. The amount of water produced when using 1, 3, and 5 effects was recorded. The most notable results were: maximum water yield reached 1.93 kg/m2 h at 1000 W/m2, at which the solar to vapor conversion efficiency was 107%. The daily water yields throughout the year were estimated, and the maximum production was 10.16 kg/m2 during a day in June, when the global horizontal irradiance was 7.01 kWh/m2. The results were also compared with other distillation systems.
One of the most important issues that directly affects human life is the lack of clean water. In 2019, it was reported that 1 in 3 people globally do not have access to safe drinking water [1]. Such a problem motivated researchers to develop different methods and technologies for water desalination, including thermal, membranes, and other advanced technologies [2]. This research focused on water distillation using thermal energy, due to its simple installation, low maintenance cost, and the abundance of solar energy that can be used for distillation [3]. However, solar stills have the disadvantage of low water output [4], so many researchers seek to create different designs for stills, such as pyramidal, spherical, or double-slope, or add other elements to conventional stills, such as spraying nozzles [5], jute, mirrors, or phase change materials (PCM) [6]. Researchers are also trying to design hybrid distillation systems by adding a parabolic reflector for the purpose of increasing the concentration of solar radiation [7], adding a flat-plate collectors [8], or utilizing the waste heat of an electricity generator for the purpose of heating the seawater before it enters the solar still.
The multiple effects diffusion solar still is distinguished from the previous types in that it reutilizes the heat gained for evaporation in the first stage to evaporate another amount of water in subsequent stages, each consisting of an evaporator and a condenser. Due to this heat reutilization, an increase in the total water output occurs. This distiller can be in a vertical or horizontal position. The following subsection summarizes several studies of both vertical and horizontal distillers.
Fukuia et al. [9] studied horizontal diffusion solar still (DSS) coupled with long wicks. They absorb seawater to their evaporating zones by capillary force. The resulted vapor diffuses and condenses on facing wicks, which drives the water to storage bags. They noticed that evaporation rates from wicks decreased as the number of effects increased. They predicted water yield of 15 kg/m2 day at 22 MJ/m2 day for 6 effects. Tanaka [10] experimentally studied vertical 6-effects DSS with gap distance of 5 mm. The unit was coupled with a flat plate reflector. The maximum productivity reached 13.4 kg/m2 day at average solar radiation of 21.55 MJ/m2. Tanaka and Iishi [11] conducted an experimental study on vertical single-effect DSS coupled with a tilted wick still. The main objective of this design was to efficiently utilize the solar energy without using a sun tracker. The maximum water yield was 4.88 kg/m2 day at 18.4 MJ/m2 day on the still surface. Park et al. [12] experimentally studied hybrid solar still consisting of 11-effects DSS coupled with single slope basin type solar still. The seawater inside the basin was heated by solar energy as well as the rejected heat from an electricity generator by adding a heat exchanger inside the basin. The maximum water productivity was 18.02 kg/m2 day at 22.37 MJ/m2 day. Lim et al. [13] conducted a 2D numerical study to examine the performance of an 11-effects DSS. The gap distance was fixed at 5 mm. They found highest water yields of 7.32-7.80 kg/m2 day during summer solstice. However, in spring/autumn equinoxes, the water yields were around 2.93-3.17 kg/m2 day. The lowest water yield was in the winter where it dropped to 0.33-0.34 kg/m2 day. Huang et al. [14] designed and implemented a novel 6-effects concentric configuration DSS with a thermal concentrator. The highest water yield was 2.2 kg/m2 h at 1000 W/m2 and three times the thermal concentration. Sharon et al. [15] conducted a numerical study on vertical DSS with a variable number of diffusion chambers ranged from 1 to 10 at variable solar intensities (100 to 1000) W/m2. They showed that the three diffusion chambers configuration was cost effective. The annual average yield was 11.13 kg/m2 day. Xu et al. [16] showed that vertical 10-effects DSS was able to reach a production rate of 5.78 L/m2 h with well-insulated side walls and glass cover.
The aim of this research was to study horizontal DSS. Specifically, studying the effect of the heat input (400, 700, and 1000 W/m2) and the number of stages (1, 3, and 5) on water yield.
The horizontal multiple effects solar still consists of several layers as in Figure 1. The first layer is a glass cover. It is originally used to transmit sunlight and reduce heat loss from the air below it. In this research, the experiments were not conducted under sunlight. Instead, an electric heating pad was used to simulate sunlight. The second layer below the glass cover is the heating pad. A thermal conductor (aluminum sheet) is glued to the bottom of the thermal pad. Attached to the aluminum sheet is a wick. The sea water is continuously driven to the drier (less saturated) regions of the wicks by means of capillary action, as in Figure 1. When the temperature of the heating pad rises, the heat is transferred to the aluminum sheet (which acts as an evaporator) and then to the wick, whereby the seawater begins to evaporate. The water vapor travels over a distance to another wick located at the bottom and attached to another aluminum sheet (acting as a condenser). The heat of the water vapor is transferred to the condenser, so the water vapor condenses, and the wick absorbs this water and transfers it to the freshwater collection container, as in Figure 2. The heat gained by the condenser is either dissipated, and the device is then considered as "single effect", or it can be used again, by transferring the heat to another wick that is attached under the condenser and saturated with sea water. For this stage, the sheet is considered as an evaporator. The process of evaporation and condensation is repeated, in a manner similar to what was mentioned earlier. The device is then considered as "multiple stages" or "multiple effects" [9,17].
The distillation unit used in conducting the experiments consists of several parts, as shown in Figure 3. The parts shown in black were 3D printed out of PETG material with 25% infill. The upper cover was made of 4 mm-thick glass and had an area of (10 × 10) cm2 (Figure 3a), and this area was fixed for all subsequent elements. The side wall thickness was 17 mm. Below the glass cover was the electric heating pad, which was 3 cm away (Figure 3b). A 0.5 mm-thick aluminum sheet was attached to the bottom of the heater. It was used as a heat conductor and evaporator for the seawater that collected in the wick at the bottom of the sheet. The used wick was a disposable towel (Cosma Belle) and was approximately 0.25 mm thick (Figure 3c). Directly under the wick was a two-post spacer (Figure 3d). The first function was to keep the seawater-saturated wick firmly attached to the aluminum sheet (evaporator) and prevent the middle of the wick from sagging downward. This was accomplished with a hexagonal mesh that held the wick and, at the same time, allowed the water vapor to pass through. The thickness of the mesh was 1 mm. The second function of the spacer was to maintain a distance of 6 mm between the seawater-saturated wick and the clean water wick. An aluminum sheet (Figure 3e) was located at the bottom of the wick collecting clean water (it was considered a condenser in this stage and an evaporator in the next stage) to which heat was transferred, causing the vapor to condense and be collected as clean water in a way that will be explained later. It should be noted that both types of wicks were wetted by deionized water before installation and were installed in perpendicular position as previously shown in Figures 1 and 2. Below the condenser-evaporator sheet, the following elements were repeated: seawater collecting wick-spacer-clean water collecting wick-condenser-evaporator sheet, and this assembly was considered as another stage/effect. At the end of the stages, a finned condenser was installed (Figure 3f) with a base thickness of 4 mm and a fin length of 26 mm. Most of these fins were immersed in seawater for the purpose of enhancing heat dissipation.
Experiments were conducted as shown in Figure 4. A tub was filled with 30 liters of water and approximately 1 kg of salt was added, raising the total dissolved solids (TDS) to more than 33, 000 ppm in order to simulate seawater (Figure 4f). The studied range of stages was 1, 3, and 5 effects. The distillation unit (Figure 4d) was assembled with a certain number of stages then positioned in a way that allowed the last finned condenser to be mostly immersed in water. Then the seawater-absorbing wick was dipped in water from both ends (one end is shown in Figure 4e, while the other end is not visible). The heat input of the electric pad heater was adjusted to a certain value with a power supply (Figure 4i). The studied range of the heat inputs was 400, 700, and 1000 W/m2, and they were determined by Eq 1 [18].
qheater=V IA | (1) |
where qheater is the selected heat input, V is the voltage, I is the current, and A is the aperture area (10 × 10) cm2. Both voltage and current were determined by trial and error, and it was noticed that they decreased as the temperature inside the unit increased, which required fine tuning of the DC power supply during the experiment until a steady state was reached (dT/dt ≈ 0).
After the power supply was set to a certain value, the temperatures inside the system began to rise and were measured using five K-type thermocouple sensors. The measurements were shown in real time on mini liquid crystal displays (Figure 4h). The temperature measurements included: glass surface from the outside Tg, the electric heating pad Th, the last finned condenser Tc, the feed water Tw, and the ambient temperature Tamb (Figure 4g).
The wicks that collected water had two ends (one of them is labeled in Figure 4b). This end was placed between several layers of dry paper tissues that absorbs moisture, and was changed after reaching steady state. These tissues were placed in a plastic container whose weight was measured by a 0.1 g-accuracy weight scale before and after the experiment (Figure 4c), where the weight difference equaled the amount of clean water produced. The tissues were covered with a plastic cover to reduce evaporation of the collected water (Figure 4a).
Due to the small size of the distillation unit, the water yield from it during the experiment period was very small, and this caused difficulty in measuring the total dissolved solids (TDS). Therefore, after measuring the weight of the resulting water, which in the worst cases was not less than 2 g at 400 W/m2 and with single effect configuration, deionized water was added to the resulted water, then both weight and TDS were measured. The initial TDS of the water was then calculated using Eq 2.
miTDSi=mfTDSf | (2) |
where mi is the mass of water resulting from the distillation unit, TDSi is the total dissolved solids of the resulted water from the distillation unit (to be calculated), mf is the mass of resulted water plus the added deionized water, and TDSf is the total dissolved solids of the resulted water plus the added deionized water.
Many researchers agree on a method to calculate the solar to vapor conversion efficiency as shown in Eq 3 [19]:
Solar to Vapor Conversion Efficiency=˙mhfgqHeaterAτ α | (3) |
where ˙m is the mass of collected water during 1 hour, hfg is the latent heat of vaporization [20], which was fixed at 2453.5 kJ/kg for feed water at 20 ℃. τ is the glass cover transmittance, which is assumed to be 0.9, and α is the absorbance of a black absorber, which is assumed to be 0.9. Previously, some researchers would multiply the optical concentration factor by the denominator terms [21,22,23], however, in this work, it is considered as one.
The daily amount of water produced during the year 2022 was estimated based on the average solar radiation during a month. Solar radiation data for the city of Dhahran in Saudi Arabia were obtained from the Prediction of Worldwide Energy Resources website of the National Aeronautics and Space Administration (NASA) [24]. Figure 5 represents the monthly average of daily global horizontal irradiance (GHI) or all sky surface shortwave downward irradiance for the months of the year. These data were used in Eq 4 [13].
Daily Water Yield[kgm2day]=GHI[kWhm2day]·τ·α·Water Yield[kgkWh] | (4) |
Water Yield[kgkWh]=˙m[kg/m2h]qHeater[W/m2]∗1000WkW | (5) |
where GHI is the global horizontal irradiance, τ is the glass cover transmittance, which is assumed to be 0.9, and α is the absorbance of a black absorber, which is assumed to be 0.9.
At the beginning of the experiments, it was observed that the temperature of both the heater and the glass cover increased rapidly, but after that it began to slow down until the system reached a steady state approximately an hour after the start of the experiment, as shown in Figure 6. The figure shows the temperatures of the glass cover Tg, heater Th, last condenser Tc, feed water Tw, and ambient Tamb.
The average temperatures for all experiments were calculated along with their standard deviations at steady state. The ambient temperature in all experiments was 21.5 ± 1.1 ℃. The temperature of the feed water for all experiments was 20.6 ± 0.9 ℃. The temperature of the final condenser for all experiments was 23.7 ± 2.1 ℃. Temperatures of the heater and glass cover in all experiments are shown in Figure 7.
It was noticed in both Figure 7a, b that the temperatures of both the heater and the glass cover were steadily increasing. For example, when the heat input was set at 400 W/m2, it was observed that temperatures rose with the increase of the number of effects. However, when the number of effects was fixed at 1, the temperature increased with the increase in the heat input. Nevertheless, when changing both the heat input and the number of effects, it was noted that the heater temperature at 5 effects and 700 W/m2 exceeded itself when the heat input was 1000 W/m2 with a one-effect configuration. In general, the high temperature of the heater was considered an advantage, as it contributed to more evaporation. Whereas, high temperature of the glass cover was considered as a disadvantage, as this indicated the presence of heat loss and poor insulation.
An experiment was conducted with 3-effects configuration and a heat input of 1000 W/m2 for 4 hours. A photo was taken after the end of the experiment showing the first seawater collecting wick (Figure 8a) with accumulated salt over approximately one-third the area of the wick. The accumulated salt was colored in blue for the ease of view. It was observed that most of the clumped salt dissolved within less than 10 hours from the end of the experiment.
When another experiment was conducted with a 3-effects configuration and a heat input of 700 W/m2 for 4 hours, salt accumulation was observed over an area of approximately 20% of the wick (Figure 8b). However, when the heat input was 400 W/m2, no salt accumulation was observed. The mean value of TDS measurements of the product for all experiments was 5000 mg/L. The maximum value was 7000 mg/L, while the minimum was 3000 mg/L.
Figure 9 shows the water yield per square meter per hour against the different heat inputs for the studied effects 1, 3, and 5. When focusing on the single effect configuration, one can notice a continuous increase in water yield, as it was 0.2 kg/m2 h at 400 W/m2 (this was the lowest value among all the experiments) and then reached 0.74 kg/m2 h at 1000 W/m2. The same behavior can be observed when focusing on the configuration of three effects as well as five effects. The water yield for the five-effects configuration was observed to be the highest among all the experiments at 1000 W/m2, which reached 1.93 kg/m2 h. However, when comparing the number of effects and the heat input for all experiments, it can be noted that the water yield of the five-effects configuration was superior to the single effect at 700 W/m2. Likewise, it can be seen that the water yield of the three-effect configuration at 700 W/m2 was superior to the single effect at 1000 W/m2. Also, it can be observed that the yield of the five-effects configuration at 700 W/m2 was close to that of three effects at 1000 W/m2. In general, it can be concluded from Figure 9 that increasing the number of effects and increasing the heat input are directly proportional to the water yield. Some of these results could be compared with other systems. For example, Kabeel [25] conducted experiments on double-slope, concave single basin and reached a maximum water yield of 0.5 kg/m2 h at 700 W/m2. Also, Li et al. [26] fabricated a foldable graphene oxide film which was used as an absorber. The water yield reached 1.45 kg/m2 at 1 kW/m2 with four orders salinity decrement, and they outperformed the TDS value of the product in this work (4500 ppm). Ghasemi et al. [20] developed a double-layer structure consisting of a carbon foam layer supporting an exfoliated graphite layer. The maximum evaporation rate was 1.2 kg/m2 h at 1 kW/m2.
Regarding the solar-vapor conversion efficiency, Figure 10 shows the percentage of conversion efficiency against heat input for all studied effects. When looking at the single-effect configuration, it was noted that the conversion efficiency was the lowest at 28%, 39%, and 41% at 400, 700, and 1000 W/m2, respectively. In the case of the three-effects configuration, the conversion efficiency was 65%, 83%, and 81% at 400, 700, and 1000 W/m2, respectively. As for the five-effects configuration, it was the highest efficiency among the configurations, reaching 84%, 106%, and 107% at 400, 700, and 1000 W/m2, respectively. A comparison of the results with other systems can be seen in Figure 10. The solar to vapor efficiency achieved by Ghasemi et al. [20] was 64% at 1000 W/m2. Kabeel [25] reached 45%, while Li et al. [26] reached 80%. However, it is expected that when insulation is improved, this percentage will increase, which will raise the water yield to a value exceeding 1.47 kg/m2 h, which was achieved by the 3-effects configuration (Figure 9). It is also important to compare the results of this work with other results regarding multiple effects distillation, whether vertical or horizontal, as shown in Table 1.
Reference | Description | Water yield | Notes |
This work | Horizontal 5-effects diffusion solar still (DSS) | Avg: 1.79 kg/kWh Max: 1.93 kg/kWh |
Avg product TDS = 4500 mg/L Thermal eff. = 107% |
Tanaka [10] | Vertical 6-effects DSS coupled with a flat plate reflector | 2.22 kg/kWh | Tap water 13.3 kg/m2 day @ 21.55 MJ/m2 day |
Fukuia et al. [9] | Horizontal 6-effects DSS | 2.45 kg/kWh | 15 kg/m2 day @ 22 MJ/m2 day |
Tanaka and Iishi [11] | Vertical 1-effect DSS coupled with a tilted wick still | 0.95 kg/kWh | 4.88 kg/m2 day @ 18.4 MJ/m2 day Thermal eff. = 55% |
Park et al. [12] | Vertical multiple effects DSS coupled with basin solar still with heated seawater | 2.90 kg/kWh | 18.02 kg/m2 h @ 22.37 MJ/m2 day |
Huang et al. [14] | Vertical 6-effects cylindrical DSS with thermal concentration | 2.20 kg/kWh | 2.20 kg/m2 h @ 1 kW/m2 |
It can be noted that the key indexes of present DSS were not superior to some of those reported in literatures. The possible reasons could be due to low ambient temperature during the experiments, which contributes to heat loss, or poor insulation, as Zhang et al. [27] noticed that side wall insulation was a major parameter in efficiency optimization. Another source of heat loss is the extended wicks that carry the condensed warm water out of the device. Moreover, this study was carried out without using extra elements such as reflectors or concentrators.
Table 2 represents a summary of all the experiments presented in the previous Figure 9, in addition to calculating the average water yield per kWh for each configuration, on which daily water yield was estimated for all months of the year.
No. of effects | Heat input [W/m2] | Actual water yield [kg/m2 h] | Water yield per kWh [kg/kWh] | Average water yield per kWh* [kg/kWh] |
One | 400 | 0.2 | 0.5 | 0.65 |
700 | 0.5 | 0.71 | ||
1000 | 0.74 | 0.74 | ||
Three | 400 | 0.47 | 1.18 | 1.38 |
700 | 1.05 | 1.50 | ||
1000 | 1.47 | 1.47 | ||
Five | 400 | 0.61 | 1.53 | 1.79 |
700 | 1.34 | 1.91 | ||
1000 | 1.93 | 1.93 | ||
* These values were used in the estimation of the daily water yield (kg/m2 day). |
Figure 11 shows the anticipated daily water yield and global horizontal irradiance during the months of 2022 for the city of Dhahran in Saudi Arabia. It can be noted that the maximum daily solar irradiance was in June, where it reached 7.01 kWh/m2 day, while the lowest value was 3.25 kWh/m2. It is become known that heat input has a significant impact on water yield, as was explained in Figure 9. Thus, it can be observed that water yields were varying for each of the three studied configurations. When we look at the month of June, we find that the water yields were 3.70, 7.85, and 10.16 kg/m2 day for each of 1, 3, and 5 effects, respectively, and these yields were the highest of the year. However, when looking at December, it can be seen that the yields dropped to 1.71, 3.64, and 4.71 kg/m2 day, which correspond to 1, 3, and 5 effects, respectively, and these yields were the lowest of the year.
In this work, a horizontal still diffusion solar device was designed and fabricated using a 3D printer. The device contained a number of layers, including: A glass cover that reduced heat dissipation, evaporators, spacers that kept the wick attached to the evaporator and allowed vapor to diffuse, then condensates. Also, some of the wicks were used to absorb seawater by capillary forces to be evaporated by the evaporator, and some of the other wicks were attached to the condenser, where the wicks were used to drive the condensed water into collectors.
In general, two parameters were studied in this research: input heat and the number of effects/stages. The range of input heat was 400, 700, 1000 W/m2, and the range of the effects studied was 1, 3, and 5 effects. The total dissolves solids (TDS) of the seawater were 33, 000 ppm. The most notable results were:
• The highest water yield was 1.93 kg/m2 h at 5 effects and 1000 W/m2 at steady state.
• The minimum water yield was 0.5 kg/m2 h at single effect and 400 W/m2 at steady state.
The average TDS of the resulting water was 4500 ppm. Although this device does not meet WHO standards for drinking water, it has shown good salinity reduction. The distillation process can be done in two stages or can be used as a pretreatment stage for other distillation techniques.
As for the average water produced per kWh, it was:
• 1.79 kg/kWh at 5 effects
• 1.38 kg/kWh at 3 effects
• 0.65 kg/kWh at single effect
The daily water yield was also estimated throughout the year in the city of Dhahran, Saudi Arabia, for all effects studied. The maximum production for five effects was 10.16 kg/m2 day in June, while the lowest yield for the same effects was 4.71 kg/m2 day in December.
The author declares that he has not used artificial intelligence (AI) tools in the creation of this article.
The author declares no conflicts of interest.
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1. | Ernest C. Nwosu, Chibuike Ononogbo, Godswill N. Nwaji, Nnamdi V. Ogueke, Emmanuel E. Anyanwu, Solar-thermal desalination in multi-stage units: a detailed review, 2025, 1573-2975, 10.1007/s10668-025-06044-3 |
Reference | Description | Water yield | Notes |
This work | Horizontal 5-effects diffusion solar still (DSS) | Avg: 1.79 kg/kWh Max: 1.93 kg/kWh |
Avg product TDS = 4500 mg/L Thermal eff. = 107% |
Tanaka [10] | Vertical 6-effects DSS coupled with a flat plate reflector | 2.22 kg/kWh | Tap water 13.3 kg/m2 day @ 21.55 MJ/m2 day |
Fukuia et al. [9] | Horizontal 6-effects DSS | 2.45 kg/kWh | 15 kg/m2 day @ 22 MJ/m2 day |
Tanaka and Iishi [11] | Vertical 1-effect DSS coupled with a tilted wick still | 0.95 kg/kWh | 4.88 kg/m2 day @ 18.4 MJ/m2 day Thermal eff. = 55% |
Park et al. [12] | Vertical multiple effects DSS coupled with basin solar still with heated seawater | 2.90 kg/kWh | 18.02 kg/m2 h @ 22.37 MJ/m2 day |
Huang et al. [14] | Vertical 6-effects cylindrical DSS with thermal concentration | 2.20 kg/kWh | 2.20 kg/m2 h @ 1 kW/m2 |
No. of effects | Heat input [W/m2] | Actual water yield [kg/m2 h] | Water yield per kWh [kg/kWh] | Average water yield per kWh* [kg/kWh] |
One | 400 | 0.2 | 0.5 | 0.65 |
700 | 0.5 | 0.71 | ||
1000 | 0.74 | 0.74 | ||
Three | 400 | 0.47 | 1.18 | 1.38 |
700 | 1.05 | 1.50 | ||
1000 | 1.47 | 1.47 | ||
Five | 400 | 0.61 | 1.53 | 1.79 |
700 | 1.34 | 1.91 | ||
1000 | 1.93 | 1.93 | ||
* These values were used in the estimation of the daily water yield (kg/m2 day). |
Reference | Description | Water yield | Notes |
This work | Horizontal 5-effects diffusion solar still (DSS) | Avg: 1.79 kg/kWh Max: 1.93 kg/kWh |
Avg product TDS = 4500 mg/L Thermal eff. = 107% |
Tanaka [10] | Vertical 6-effects DSS coupled with a flat plate reflector | 2.22 kg/kWh | Tap water 13.3 kg/m2 day @ 21.55 MJ/m2 day |
Fukuia et al. [9] | Horizontal 6-effects DSS | 2.45 kg/kWh | 15 kg/m2 day @ 22 MJ/m2 day |
Tanaka and Iishi [11] | Vertical 1-effect DSS coupled with a tilted wick still | 0.95 kg/kWh | 4.88 kg/m2 day @ 18.4 MJ/m2 day Thermal eff. = 55% |
Park et al. [12] | Vertical multiple effects DSS coupled with basin solar still with heated seawater | 2.90 kg/kWh | 18.02 kg/m2 h @ 22.37 MJ/m2 day |
Huang et al. [14] | Vertical 6-effects cylindrical DSS with thermal concentration | 2.20 kg/kWh | 2.20 kg/m2 h @ 1 kW/m2 |
No. of effects | Heat input [W/m2] | Actual water yield [kg/m2 h] | Water yield per kWh [kg/kWh] | Average water yield per kWh* [kg/kWh] |
One | 400 | 0.2 | 0.5 | 0.65 |
700 | 0.5 | 0.71 | ||
1000 | 0.74 | 0.74 | ||
Three | 400 | 0.47 | 1.18 | 1.38 |
700 | 1.05 | 1.50 | ||
1000 | 1.47 | 1.47 | ||
Five | 400 | 0.61 | 1.53 | 1.79 |
700 | 1.34 | 1.91 | ||
1000 | 1.93 | 1.93 | ||
* These values were used in the estimation of the daily water yield (kg/m2 day). |